{"id":83236,"date":"2000-04-02T00:00:00","date_gmt":"2000-04-02T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudios-sobre-geoides-terrestres-y-marinos\/"},"modified":"2000-04-02T00:00:00","modified_gmt":"2000-04-02T00:00:00","slug":"estudios-sobre-geoides-terrestres-y-marinos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudios-sobre-geoides-terrestres-y-marinos\/","title":{"rendered":"Estudios sobre geoides terrestres y marinos"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gema Rodriguez Velasco <\/strong><\/h2>\n<p>Se presenta un estudio sobre distintas metodolog\u00edas de determinaci\u00f3n de geoide gravim\u00e9trico, con especial inter\u00e9s en las \u00e1reas que incluyen zonas terrestres y marinas.  para ilustrar estos estudios se calculan distintos resultados de geoides sobre una zona del este de la pen\u00ednsula ib\u00e9rica y oeste del mar mediterr\u00e1neo y se analiza su sensibilidad a distintos factores empleados en el c\u00e1lculo.  se presenta un an\u00e1lisis de t\u00e9cnicas de sat\u00e9lites altim\u00e9tricos para determinaci\u00f3n del campo de la gravedad.  sobre zonas de aguas someras, resulta preferible la determinaci\u00f3n de geoides puramente gravim\u00e9tricos, mientras que los datos de altimetr\u00eda son m\u00e1s \u00fatiles para la determinaci\u00f3n de la superficie media del mar. En combinaci\u00f3n con un geoide de precisi\u00f3n se podr\u00e1 as\u00ed obtener medelos locales de superficie topogr\u00e1fica del mar.  por \u00faltimo se demuestra la importante correlaci\u00f3n existente en este tipo de \u00e1reas entre esta superficie y la batimetr\u00eda del fondo. De este modo, es f\u00e1cilmente modelable por funciones de la profundidad.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudios sobre geoides terrestres y marinos<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudios sobre geoides terrestres y marinos <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gema Rodriguez Velasco <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 04\/02\/2000<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li> Sevilla De Lerma Miguel J.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: elisa Buforn peir\u00f3 <\/li>\n<li> Martinez benjamin Juan  Jos\u00e9 (vocal)<\/li>\n<li>n. Tziavos ilias (vocal)<\/li>\n<li> Nu\u00f1ez del pozo alfonso (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gema Rodriguez Velasco Se presenta un estudio sobre distintas metodolog\u00edas de determinaci\u00f3n de geoide gravim\u00e9trico, con especial [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,2265,31013,105567],"tags":[28557,176519,57617,176520,154366,50254],"class_list":["post-83236","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geodesia","category-geodesia-de-satelites","category-geodesia-fisica","tag-elisa-buforn-peiro","tag-gema-rodriguez-velasco","tag-Martinez-benjamin-juan-jose","tag-n-tziavos-ilias","tag-nunez-del-pozo-alfonso","tag-sevilla-de-lerma-miguel-j"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/83236","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=83236"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/83236\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=83236"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=83236"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=83236"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}